These similarities include similar mineralization ages (ca. ~140 Ma), ore-related alteration styles, ore mineral assemblages, ore host and possibly a magmatic-related ore-fluid source (Table 5; Su et al., 2008, 2009a, b, 2012, 2018; Cline et al., 2013; Hou et al., 2016; Chen et al., 2018). However, a key difference between the gold and …